Crystal Grottoes was discovered in 1920 in the course of quarrying operations by a roadconstruction crew trying to obtain gravel. A drill bit disappeared into a hole, and the crew realized they had found a cave. Blasting produced the entrance which is still used, and in 1922 the cave was opened to the public. A mapping operation in 1968 revealed about a half mile of passages, but only about one third of the cave is accessed during the tour, which takes about 30–35 minutes.
Geology
Crystal Grottoes is an example of a solutional cave, formed in a karst environment within a synclinal occurrence of Tomstown Dolomite. The cave is essentially horizontal throughout its extent and the passages are typically high and narrow. A great deal of brown and red clay fills most of the cave to a considerable extent; the commercial tour routes involved the removal of up to of this clay in of the passages. Sediment fills many of the undeveloped passages to within a foot or two of the ceiling, thereby making many crawlways. No streams exist in the cave, although a small "lake" or pool is maintained by drip water.
Description
Most of the rooms abound in speleothem formations, generally stalactites, flowstone, and columns. They are typically white or buff, with one area tinted a light red, by iron oxides. The first room is below the entrance house and is oblate in shape, being long, wide, and high. At each end it is pinched out by mud flows and narrowing of the passage. This room originally contained a considerable number of formations, but quarrying operations and clearing of passages have removed them except along the west wall where flowstone and stalactites are abundant. The passages are continuously lined or covered by formations. Delicate draperies, bacon, and columns predominate. The colors are generally pure white or buff with occasional deeper tints. The passages forming Fairyland are studded with stalactites and stalagmites of a delicatelight red hue. The Blanket Room is the largest room in the caverns at long and wide. Large sheets of stalactites and draperies hang in clusters from the ceiling, which is here high. The passage leading to the lake is profuse with formations and in part is bridged by flat-lying travertine, a condition that is found in many of the passages not open to the public. The lake is a small pool fed by water dripping from the ceiling. In wet seasons the water accumulates at a rate necessitating periodic bailing. The passages not open to the public are similar to those already described except they are constricted at many points. Orange-brown clay that covers the floor and lower walls of these passages is often overlain by calcareous formations. The commercial tour route covers approximately one third of the known cave.
